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  • 1
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    Equations for the dynamics of gust fronts and shock waves (1977)
    In:  CASI
    Details
    Publication Date: 2006-01-12
    Description: Equations are presented for the growth or decay rates of moving and deforming vortex sheets (gust fronts) and shock waves. The equations exhibit a cross-coupling between these two types of surface discontinuity.
    Keywords: METEOROLOGY AND CLIMATOLOGY
    Type: NASA. Goddard Space Flight Center 3d NASA Weather and Climate Program Sci. Rev.; p 225-227
    Format: text
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    NASA TECHNICAL REPORTS
  • 2
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    General solutions for the movement of storms (1977)
    In:  CASI
    Details
    Publication Date: 2006-01-12
    Description: Diagnostic solutions are presented for the displacement velocity of a storm vortex and the velocity of the centroid of the storm's convection.
    Keywords: METEOROLOGY AND CLIMATOLOGY
    Type: NASA. Goddard Space Flight Center 3d NASA Weather and Climate Program Sci. Rev.; p 219-223
    Format: text
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    NASA TECHNICAL REPORTS
  • 3
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    Formulas for determining storm movement from the surrounding fields (1979)
    In:  CASI
    Details
    Publication Date: 2016-06-07
    Description: Formulas are given for determining a conserved property of a storm and its centroid from an scalar field that has a tendency equation. The velocity of the centroid is also given. These formulas depend only on fields that are external to the storm.
    Keywords: METEOROLOGY AND CLIMATOLOGY
    Type: NASA. Goddard Space Flight Center 4th NASA Weather and Climate Program Sci. Rev.; p 37-40
    Format: application/pdf
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    NASA TECHNICAL REPORTS
  • 4
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    Wind-tunnel tests and computer simulations of buoyant wing-tip vortices (1974)
    In:  Other Sources
    Details
    Publication Date: 2019-07-13
    Description: It is demonstrated that wing-tip vortices with buoyant cores can be made in a wind tunnel. Wing-tip vortices generated by an aircraft often become buoyant, because of heating effects due to the jet exhaust or in connection with a descending motion in a stable atmosphere. A description of wind-tunnel studies is given, taking into account the experimental conditions, the transition to turbulence, and the drift of the buoyant vortex. A computer simulation of wing-tip vortices is also discussed.
    Keywords: AERODYNAMICS
    Type: Conference on Aerospace and Aeronautical Meteorology; Nov 12, 1974 - Nov 15, 1974; El Paso, TX
    Format: text
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    NASA TECHNICAL REPORTS
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